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Slip Distribution of the 1963 Great Kurile Earthquake Estimated from Tsunami Waveforms

机译:根据海啸波形估算的1963年千岛地震的滑动分布

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The 1963 great Kurile earthquake was an underthrust earthquake occurred in the Kurile–Kamchatka subduction zone. The slip distribution of the 1963 earthquake was estimated using 21 tsunami waveforms recorded at tide gauges along the Pacific and Okhotsk Sea coasts. The extended rupture area was divided into 24 subfaults, and the slip on each subfault was determined by the tsunami waveform inversion. The result shows that the largest slip amount of 2.8 m was found at the shallow part and intermediate depth of the rupture area. Large slip amounts were found at the shallow part of the rupture area. The total seismic moment was estimated to be 3.9 × 1021 Nm (Mw 8.3). The 2006 Kurile earthquake occurred right next to the location of the 1963 earthquake, and no seismic gap exists between the source areas of the 1963 and 2006 earthquakes.
机译:1963年的库里尔大地震是在库里尔-堪察加俯冲带发生的一次逆冲地震。 1963年地震的滑动分布是使用沿太平洋和鄂霍次克海沿岸潮汐仪记录的21个海啸波形估算的。扩展的破裂区域被划分为24个子断层,每个子断层的滑动由海啸波形反演确定。结果表明,在破裂区的浅部和中深度发现最大的滑动量为2.8 m。在破裂区域的浅部发现大量的滑移。总地震矩估计为3.9×1021 Nm(Mw 8.3)。 2006年的库利尔地震发生在1963年地震发生的位置附近,并且在1963年地震和2006年地震的震源区之间没有地震间隔。

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